Alkanes in Quaternary deposits of the Laptev Sea

E. A. Romankevich, A. A. Vetrov, N. A. Belyaev, V. I. Sergienko, I. P. Semiletov, S. V. Sukhoverkhov, S. Yu Bratskaya, N. A. Prokuda, A. S. Ulyantsev

Arctic Seas Carbon Research Internatonal Lab

Research output: Contribution to journal › Article › peer-review

3 Citations (Scopus)

Abstract

The distribution and genesis of n-alkanes in sediments from the 38-m sequence obtained during core boring in the Ivashkina lagoon were studied. Sediments were formed in the Holocene as a result of thermokarst and penetration of seawater. The sequence mostly includes permafrost rocks partially molten in the upper horizons and covered by Quaternary deposits, which are mostly the products of thermoabrasion.

Original language	English
Pages (from-to)	36-39
Number of pages	4
Journal	Doklady Earth Sciences
Volume	472
Issue number	1
DOIs	https://doi.org/10.1134/S1028334X17010093
Publication status	Published - 1 Jan 2017

ASJC Scopus subject areas

Earth and Planetary Sciences (miscellaneous)
Earth and Planetary Sciences(all)

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title = "Alkanes in Quaternary deposits of the Laptev Sea",

abstract = "The distribution and genesis of n-alkanes in sediments from the 38-m sequence obtained during core boring in the Ivashkina lagoon were studied. Sediments were formed in the Holocene as a result of thermokarst and penetration of seawater. The sequence mostly includes permafrost rocks partially molten in the upper horizons and covered by Quaternary deposits, which are mostly the products of thermoabrasion.",

author = "Romankevich, {E. A.} and Vetrov, {A. A.} and Belyaev, {N. A.} and Sergienko, {V. I.} and Semiletov, {I. P.} and Sukhoverkhov, {S. V.} and Bratskaya, {S. Yu} and Prokuda, {N. A.} and Ulyantsev, {A. S.}",

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AU - Romankevich, E. A.

AU - Vetrov, A. A.

AU - Belyaev, N. A.

AU - Sergienko, V. I.

AU - Semiletov, I. P.

AU - Sukhoverkhov, S. V.

AU - Bratskaya, S. Yu

AU - Prokuda, N. A.

AU - Ulyantsev, A. S.

PY - 2017/1/1

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AB - The distribution and genesis of n-alkanes in sediments from the 38-m sequence obtained during core boring in the Ivashkina lagoon were studied. Sediments were formed in the Holocene as a result of thermokarst and penetration of seawater. The sequence mostly includes permafrost rocks partially molten in the upper horizons and covered by Quaternary deposits, which are mostly the products of thermoabrasion.

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